17O和29Si的NMR参数MgSiO3阶段的高分辨率固态NMR光谱和第一个原则计算的高分辨率固态NMR光谱
Sharon E Ashbrook1, Andrew J Berry, Daniel J Frost
1School of Chemistry and EaStCHEM, University of St Andrews, North Haugh, St Andrews KY16 9ST, U.K. sema@st-andrews.ac.uk
这项研究详细介绍了六种酸 (MgSiO3) 多态的29Si和17O NMR参数. 这些发现澄清了地球上氧气地点的分配.
科学领域:
- 地质化学和材料科学 材料科学
- 固态核磁共振 (NMR) 光谱学 固态核磁共振 (NMR) 光谱学
- 计算材料科学科学 计算材料科学
背景情况:
- 酸 (MgSiO3) 多态是地球地幔的关键组成部分,在不同压力和温度下表现出结构转变.
- 了解这些结构对于解释地震数据和地幔组成至关重要.
研究的目的:
- 为了确定29Si和17O核磁共振 (NMR) 的参数,六个MgSiO3多态.
- 在低压多态体中分配氧位点,并为高压多态体提供第一个17O NMR数据.
- 为了将NMR参数与局部结构变异相关联.
主要方法:
- 高分辨率的固态NMR光谱,包括三次量子魔术角度旋转 (MAS),多次量子MAS (MQMAS) 和卫星过渡MAS (STMAS) 实验.
- 使用测量仪的第一原则计算,包括带有周期边界条件的投影机增强波 (GIPAW) 形式主义.
- 对29Si和17ONMR化学转移和四极性参数的分析.
主要成果:
- 解决并分配了170个NMR光谱中的所有氧物种,用于ortho-,clino-和protoenstatite,与以前的分配不同.
- 提交了第一个17ONMR数据,用于多数石, akimotoite和perovskite,证实了之前的29SiNMR发现.
- 证明17O化学转移与Si-O键长度相关,但也受到协调环境的影响.
结论:
- 该研究为MgSiO3多态体提供了明确的17O NMR赋值,这对于理解地球地幔结构至关重要.
- 核磁共振参数提供了关于MgSiO3.3中局部结构,协调和结合之间的关系的见解.
- 这项工作为在地球科学中使用NMR探测高压矿物相奠定了基础.
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